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4.5 The Theory of Plate Tectonics
4.5 The Theory of Plate Tectonics

... continents similar to those on the ocean floor. ...
Answers - MrTubb
Answers - MrTubb

... 15. Earth's surface is constantly changing. Volcanoes erupt and form new crust. Lithospheric plate motions bend and crack old crust and cause earthquakes. Where do most of Earth's earthquakes and volcanoes occur? A. at the center of continental plates B. at the equator C. along hot spots in oceanic ...
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No Slide Title

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... travel through solid rock and fluids, like water or the liquid layers of the Earth. They push and pull the rock they travel through. Subjected to a P wave, particles move in the same direction that the wave is moving in, which is the direction that the energy is travelling in. As they pass, rocks ar ...
Document
Document

... location of a divergent boundary, also is a hot spot. But others, such as the Hawaiian Islands, are found well within tectonic plate boundaries. These hot spots are isolated and not associated with spreading centers or subduction zones. The cause of hot spots is believed to be plumes of motlen rock ...
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Large igneous province



A large igneous province (LIP) is an extremely large accumulation of igneous rocks, including liquid rock (intrusive) or volcanic rock formations (extrusive), when hot magma extrudes from inside the Earth and flows out. The source of many or all LIPs is variously attributed to mantle plumes or to processes associated with plate tectonics. Types of LIPs can include large volcanic provinces (LVP), created through flood basalt and large plutonic provinces (LPP). Eleven distinct flood basalt episodes occurred in the past 250 million years, creating volcanic provinces, which coincided with mass extinctions in prehistoric times. Formation depends on a range of factors, such as continental configuration, latitude, volume, rate, duration of eruption, style and setting (continental vs. oceanic), the preexisting climate state, and the biota resilience to change.
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